Analysis reveals the structure of rare-earth elements in marine sediments, highlighting their storage potential.
Deep-sea sediments hold large quantities of critical rare-earth elements (REE) sequestered in a defective apatite-type bonding environment within an amorphous matrix coating biogenic fluorapatite nanocrystals (Ca 5 (CO 3 ) x (PO 4 ) 3− x F 1+ x ).
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Manceau et al. (2026) studied this question.
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